Informacja

Drogi użytkowniku, aplikacja do prawidłowego działania wymaga obsługi JavaScript. Proszę włącz obsługę JavaScript w Twojej przeglądarce.

Wyszukujesz frazę "Żarski, M." wg kryterium: Autor


Wyświetlanie 1-2 z 2
Tytuł:
Znalezisko kości ssaków plejstoceńskich w Garwolinie (Nizina Mazowiecka)
Bones of Pleistocene Mammals find in Garwolin (Mazovian Lowland)
Autorzy:
Żarski, M.
Jakubowski, G.
Ploch, I.
Powiązania:
https://bibliotekanauki.pl/articles/2075105.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Garwolin
mammoth
Vistulian
mamut
Wisła
Opis:
Remains of woolly mammoth, woolly rhinoceros, bison, reindeer and horse bones were found in 2006 y in gravel pit in Wilga Valley near Garwolin. The most numerous represent the mammoth bones: fragments of skull, teeth, and pelvis with biting trace by predators. The bones were found in the fluvial sands and gravels at the depth of 5–6 m below the ground surface. Geological studies have identified the origin and age of the deposits for the period of Vistulian. The age of mammoth bones in two analysis used 14C method is between 38 and 46 ka and is correlated with the Grudziadz Interstadial. Below the Vistululian sands and gravels are located tills of the Wartanian Glaciation, and above Holocene peat.
Źródło:
Przegląd Geologiczny; 2014, 62, 10/1; 525--531
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Stratigraphy and palaeoenvironment of Stajna Cave (southern Poland) with regard to habitation of the site by Neanderthals
Autorzy:
Żarski, M.
Winter, H.
Nadachowski, A.
Urbanowski, M.
Socha, P.
Kenig, K.
Marcinkowski, B.
Krzemińska, E.
Stefaniak, K.
Nowaczewska, W.
Marciszak, A.
Powiązania:
https://bibliotekanauki.pl/articles/2060379.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Stajnia Cave
Neanderthal
Vistulian
palaeoenvironment
Częstochowa Upland
Opis:
The Stajnia Cave is one of the most important archaeological sites due to the finds of the first remains of Neanderthals in Poland, and several tens of thousands of flint artefacts from the Middle Palaeolithic. Based on geological, geochemical, palaeobotanical, palaeozoological, archaeological and isotope analyses, coupled with absolute age determinations (OSL, U-Th and C14), 15 lithostratigraphic layers were distinguished and palaeoenvironmental conditions during the sedimentation of these beds were determined. The cave loams accumulated through weathering, aeolian and fluvial processes. Their age may be correlated with an interval from the Early Glacial to the Late Pleniglacial of the Visulian (Weichselian) Glaciation. Archaeological relics related to the Neanderthals have been discovered in layer D with an absolute age of about 52,000–45,000 years BP and correlated with MIS 3 – the Middle Plenivistulian (Interplenivistulian). Climate oscillations in the Vistulian are reflected by the type of the sediments and their physical-chemical features, allowing determining warmer interstadial and colder stadial periods. Generally, the climate was cold, characteristic of tundra areas with a typical vegetation and fauna, and with the mean temperature of the warmest month not exceeding 12°C. Based on multi-proxy studies it can be concluded that from layer E1 upwards, the climate conditions became progressively drier. At that time, the climate was cold with continental features enhancing tundra domination. This conclusion is confirmed by palaeontological investigations and the record of stable oxygen isotopes in the teeth of reindeer. The studies have also indicated seasonal migration of reindeer on the tundra that surrounded the cave. Probably, short-term slight climate warmings occurred during the Middle Plenivistulian (Interplenivistulian).
Źródło:
Geological Quarterly; 2017, 61, 2; 350--369
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

    Ta witryna wykorzystuje pliki cookies do przechowywania informacji na Twoim komputerze. Pliki cookies stosujemy w celu świadczenia usług na najwyższym poziomie, w tym w sposób dostosowany do indywidualnych potrzeb. Korzystanie z witryny bez zmiany ustawień dotyczących cookies oznacza, że będą one zamieszczane w Twoim komputerze. W każdym momencie możesz dokonać zmiany ustawień dotyczących cookies